Diurnal and semidiurnal tide-induced lateral movement of Ronne Ice Shelf, Antarctica

Recent GPS observations from a spatially extensive networkacross Ronne Ice Shelf show significant daily ice flowvariations. At all sites, the almost-synchronous horizontaldisplacements occur at diurnal and semidiurnal tidal periods.During spring tides, displacements, velocities and strains nearthe i...

Full description

Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Makinson, K, King, MA, Nicholls, KW, Gudmundsson, GH
Format: Article in Journal/Newspaper
Language:English
Published: Wiley-Blackwell Publishing 2012
Subjects:
Online Access:https://doi.org/10.1029/2012GL051636
http://ecite.utas.edu.au/89656
id ftunivtasecite:oai:ecite.utas.edu.au:89656
record_format openpolar
spelling ftunivtasecite:oai:ecite.utas.edu.au:89656 2023-05-15T13:42:40+02:00 Diurnal and semidiurnal tide-induced lateral movement of Ronne Ice Shelf, Antarctica Makinson, K King, MA Nicholls, KW Gudmundsson, GH 2012 https://doi.org/10.1029/2012GL051636 http://ecite.utas.edu.au/89656 en eng Wiley-Blackwell Publishing http://dx.doi.org/10.1029/2012GL051636 Makinson, K and King, MA and Nicholls, KW and Gudmundsson, GH, Diurnal and semidiurnal tide-induced lateral movement of Ronne Ice Shelf, Antarctica, Geophysical Research Letters, 39, (10) Article L10501. ISSN 1944-8007 (2012) [Refereed Article] http://ecite.utas.edu.au/89656 Earth Sciences Geophysics Geodesy Refereed Article PeerReviewed 2012 ftunivtasecite https://doi.org/10.1029/2012GL051636 2022-09-05T22:16:43Z Recent GPS observations from a spatially extensive networkacross Ronne Ice Shelf show significant daily ice flowvariations. At all sites, the almost-synchronous horizontaldisplacements occur at diurnal and semidiurnal tidal periods.During spring tides, displacements, velocities and strains nearthe ice front have superimposed oscillations that are +-300%of their mean values and occur over a six-hour period, resultingin regular ice shelf flow reversals. Close to ice streamgrounding lines, however, the horizontal diurnal and semidiurnalsignals decay and almost vanish. From our analysis,we conclude that ice shelves respond primarily elasticallyto tidal tilting, thus accounting for the observed diurnal andsemidiurnal flow variations, and their amplification towardthe ice shelf front. Our findings suggest that detailed modelingof these data could provide improved ice shelf and icestream models for correctly simulating ice shelf flow andpredicting future ice sheet evolution. Article in Journal/Newspaper Antarc* Antarctica Ice Sheet Ice Shelf Ice Shelves Ronne Ice Shelf eCite UTAS (University of Tasmania) Ronne Ice Shelf ENVELOPE(-61.000,-61.000,-78.500,-78.500) Tilting ENVELOPE(-54.065,-54.065,49.700,49.700) Geophysical Research Letters 39 10 n/a n/a
institution Open Polar
collection eCite UTAS (University of Tasmania)
op_collection_id ftunivtasecite
language English
topic Earth Sciences
Geophysics
Geodesy
spellingShingle Earth Sciences
Geophysics
Geodesy
Makinson, K
King, MA
Nicholls, KW
Gudmundsson, GH
Diurnal and semidiurnal tide-induced lateral movement of Ronne Ice Shelf, Antarctica
topic_facet Earth Sciences
Geophysics
Geodesy
description Recent GPS observations from a spatially extensive networkacross Ronne Ice Shelf show significant daily ice flowvariations. At all sites, the almost-synchronous horizontaldisplacements occur at diurnal and semidiurnal tidal periods.During spring tides, displacements, velocities and strains nearthe ice front have superimposed oscillations that are +-300%of their mean values and occur over a six-hour period, resultingin regular ice shelf flow reversals. Close to ice streamgrounding lines, however, the horizontal diurnal and semidiurnalsignals decay and almost vanish. From our analysis,we conclude that ice shelves respond primarily elasticallyto tidal tilting, thus accounting for the observed diurnal andsemidiurnal flow variations, and their amplification towardthe ice shelf front. Our findings suggest that detailed modelingof these data could provide improved ice shelf and icestream models for correctly simulating ice shelf flow andpredicting future ice sheet evolution.
format Article in Journal/Newspaper
author Makinson, K
King, MA
Nicholls, KW
Gudmundsson, GH
author_facet Makinson, K
King, MA
Nicholls, KW
Gudmundsson, GH
author_sort Makinson, K
title Diurnal and semidiurnal tide-induced lateral movement of Ronne Ice Shelf, Antarctica
title_short Diurnal and semidiurnal tide-induced lateral movement of Ronne Ice Shelf, Antarctica
title_full Diurnal and semidiurnal tide-induced lateral movement of Ronne Ice Shelf, Antarctica
title_fullStr Diurnal and semidiurnal tide-induced lateral movement of Ronne Ice Shelf, Antarctica
title_full_unstemmed Diurnal and semidiurnal tide-induced lateral movement of Ronne Ice Shelf, Antarctica
title_sort diurnal and semidiurnal tide-induced lateral movement of ronne ice shelf, antarctica
publisher Wiley-Blackwell Publishing
publishDate 2012
url https://doi.org/10.1029/2012GL051636
http://ecite.utas.edu.au/89656
long_lat ENVELOPE(-61.000,-61.000,-78.500,-78.500)
ENVELOPE(-54.065,-54.065,49.700,49.700)
geographic Ronne Ice Shelf
Tilting
geographic_facet Ronne Ice Shelf
Tilting
genre Antarc*
Antarctica
Ice Sheet
Ice Shelf
Ice Shelves
Ronne Ice Shelf
genre_facet Antarc*
Antarctica
Ice Sheet
Ice Shelf
Ice Shelves
Ronne Ice Shelf
op_relation http://dx.doi.org/10.1029/2012GL051636
Makinson, K and King, MA and Nicholls, KW and Gudmundsson, GH, Diurnal and semidiurnal tide-induced lateral movement of Ronne Ice Shelf, Antarctica, Geophysical Research Letters, 39, (10) Article L10501. ISSN 1944-8007 (2012) [Refereed Article]
http://ecite.utas.edu.au/89656
op_doi https://doi.org/10.1029/2012GL051636
container_title Geophysical Research Letters
container_volume 39
container_issue 10
container_start_page n/a
op_container_end_page n/a
_version_ 1766171333497978880